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Journal ArticleDOI

Cyanobacteria-containing biofilms from a Mayan monument in Palenque, Mexico

TL;DR: The structural characterization and species composition of biofilms from the walls of one of the buildings at the archaeological site of Palenque, Mexico, are reported and the implications for the development and permanence of species capable of withstanding temporal heterogeneity in and on El Palacio are discussed.
Abstract: Surfaces of buildings at the archaeological site of Palenque, Mexico, are colonized by cyanobacteria that form biofilms, which in turn cause aesthetic and structural damage. The structural characterization and species composition of biofilms from the walls of one of these buildings, El Palacio, are reported. The distribution of photosynthetic microorganisms in the biofilms, their relationship with the colonized substratum, and the three-dimensional structure of the biofilms were studied by image analysis. The differences between local seasonal microenvironments at the Palenque site, the bioreceptivity of stone and the relationship between biofilms and their substrata are described. The implications for the development and permanence of species capable of withstanding temporal heterogeneity in and on El Palacio, mainly due to alternating wet and dry seasons, are discussed. Knowledge on how different biofilms contribute to biodegradation or bioprotection of the substratum can be used to develop maintenance ...

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SUPPLEMENTARY MATERIAL
Table 2. Species identified in sampling sites at El Palacio (Palenque).
Taxa Size Location Figure
Cyanobacteria
Chroococcales
Synechococcaceae
Aphanothecoideae
Aphanothece castagnei
(Bre
´
bisson) Rabenhorst
Cells 4.1-(5.3)76.6 mm wide and
2.6-(4.9)77.2 mm long
I
III
IV
Gloeothece cf. palea (Ku
¨
tz.)
Rabenhorst
Cells 2.3-(2.4)72.6 mm wide,
4.6-(7.9)711.2 mm with sheath and 2.6-
(4.9)77.26 long,
6.6-(9.2)711.8 mm with sheath.
I
II
III
IV
Microcystaceae
Gloeocapsa calcicola Gardner Cells 2.6-(3.3)74.2 mm wide and
9.2-(13.8)718.5 mm with sheath
I
II
III
IV
Gloeocapsa quaternata Ku
¨
tzing Cells 2.3-(2.9)73.5 mm wide and
3.2-(5.3)77.5 mm long. With sheath 5-
(5.7)76.5 mm wide and
6-(7.2)78.5 mm long
I
II
III
IV
Chroococcaceae
Asterocapsa divina Koma
´
rek Colonies 13.3-(63.9)7114.5 mm wide. Cells
6.6-(9.9)713.3 mm wide and 9.9-
(12.4)714.9 mm long. Cells with sheath
9.9-(25.7)741.5 mm wide
II
III
IV
Chroococcus cf. schizodermaticus
W. et G.S. West
Colonies de 7-(13.5)720 mm wide. Cells 4-
(8.5)713 mm wide and
5-(10.5)716 mm long
I
IV
Oscillatoriales
Pseudoanabaenaceae
Leptolyngbyoideae
Leptolyngbya cf. compacta
(Ku
¨
tzing ex Hansgirg) Koma
´
rek
et Anagnostidis
Filament diameter. Trichomes
1.3-(1.6)72 mm wide and cells
1.9-(2.6)73.3 mm long, sheath
1.5-(1.7)72 mm thick
I
IV
Schizotrichaceae
Schizothrix bosniaca (Hansgirg)
Geitler
Trichomes 2.4-(4.1)75.7 mm wide, cells 3.7-
(7.3)711 mm long
I
IV
(continued)

SUPPLEMENTARY MATERIAL
Table 2. (Continued).
Taxa Size Location Figure
Nostocales
Scytonemataceae
Scytonema guyanense (Mont.)
Bornet et Flahaut
Cells 4.9-(9.5)714.1 mm wide and
3.4714.9 mm long. Heterocysts 3.4-
(9.2)714.9 mm wide and
5.5-(10.8)716.1 mm long.
Sheath 8.3-(10.5)712.7 mm
I
IV
Nostocaceae
Nostoc commune Vaucher ex
Bornet et Flahaut
Cells 5.8-(6.6)77.4 mm wide and
4.9-(7.4)79.9 mm long. Heterocysts 6.6-
(7.4)78.3 mm wide and 7.4-(7.8)78.3 mm
long
I
IV
Chlorophyta
Trentepohliophyceae
Trentepohliales
Trentepohlia aurea (Linn) Martius Young cells: 3.9-(16.7)729.5 mm wide and
3.9-(13.6)723.2 mm long. Mature cells:
9.9-(18.2)726.5 mm wide and 18.2-
(35.2)752.1 mm long. Sporangia: 15.8-
(22.1)728. 2 mm wide and 17.8-
(25.5)733.2 mm long
III
IV
Citations
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Journal ArticleDOI
TL;DR: It is suggested that a standardized laboratory protocol for evaluating stone bioreceptivity and definition of a stone biOREceptivity index are required to enable creation of a database on the primary bioreCEPTivity of stone materials.

224 citations


Cites background from "Cyanobacteria-containing biofilms f..."

  • ...The state of conservation of building materials and their maintenance seems to also affect bioreceptivity (Ortega-Calvo et al., 1995; Ramirez et al., 2010; Jim and Chen, 2011)....

    [...]

  • ...Ramirez et al. (2010) reported that strong seasonal changes in rainfall and relative humidity defined a strict cyanobacterial growth sequence on a Mayanmonument in Palenque (Mexico), although bioreceptivity was also an important factor in the development of microorganisms....

    [...]

Journal ArticleDOI
TL;DR: In this article, a review of the major routes and mechanisms which led to biodeterioration, discusses current remedial methodologies and suggests future directions, and discusses current methods and solutions.
Abstract: Since ancient time, magnificence and beauty have been the goals of architecture. Artists and architects used high strength, durable and beautiful stones like marble and limestone for the construction of monuments like Taj Mahal, Milan Cathedral, Roman Catacombs and Necropolis in Rome etc. These historic monuments are exposed to open air which allows the invading army of algae, cyanobacteria, fungi etc. to easily access them. The invasion of microorganisms and their subsequent interaction with mineral matrix of the stone substrate under varied environment conditions fosters deterioration of stones by multiple mechanisms resulting in loss of strength, durability, and aesthetic appearance. The review details about the major routes and mechanisms which led to biodeterioration, discusses current remedial methodologies and suggests future directions.

120 citations


Cites background from "Cyanobacteria-containing biofilms f..."

  • ...Algae Aesthetic and chemical deterioration Biofilm formation; color alteration; black crust formation; [18,21,31,32]...

    [...]

  • ...1 Photoautotrophs Cyanobacteria Aesthetic and chemical deterioration Biofilm formation; color alteration; patina formation; crust formation; bioweathering as a consequences of calcium uptake, precipitation of calcium salt and formation of secondary minerals [17-23]...

    [...]

Journal ArticleDOI
TL;DR: The secretion of protective pigments in the polysaccharide layers, namely mycosporine amino acid-like substances (MAAs) and scytonemins, under exposure to UV radiation showed how the acclimation response contributes to the persistence of cyanobacteria on exposed lithoid surfaces in tropical areas.
Abstract: Three coccoid and two filamentous cyanobacterial strains were isolated from phototrophic biofilms exposed to intense solar radiation on lithic surfaces of the Parasurameswar Temple and Khandagiri caves, located in Orissa State, India. Based on to their morphological features, the three coccoid strains were assigned to the genera Gloeocapsosis and Gloeocapsa, while the two filamentous strains were assigned to the genera Leptolyngbya and Plectonema. Eleven to 12 neutral and acidic sugars were detected in the slime secreted by the five strains. The secretions showed a high affinity for bivalent metal cations, suggesting their ability to actively contribute to weakening the mineral substrata. The secretion of protective pigments in the polysaccharide layers, namely mycosporine amino acid-like substances (MAAs) and scytonemins, under exposure to UV radiation showed how the acclimation response contributes to the persistence of cyanobacteria on exposed lithoid surfaces in tropical areas.

98 citations


Cites background from "Cyanobacteria-containing biofilms f..."

  • ...Biofilms growing on lithic surfaces of monuments have been intensively studied over recent decades since there is growing concern for the preservation of cultural heritage (de la Torre et al. 1993; Gaylarde and Morton 1999; Ramirez et al. 2010)....

    [...]

Book ChapterDOI
01 Jan 2012
TL;DR: The distribution of particular cyanobacterial taxa on monuments in urban or agricultural areas is related mostly to climatic conditions and the position and orientation of the hard surface with respect to water availability and air circulation.
Abstract: Biofilm-forming cyanobacteria are widespread inhabitants of exposed stones in archaeological and historical sites and caves. Outdoors, these phototrophic biofilms are adapted to all types of stress imposed by growth at the air-rock interface and have developed the capacity to tolerate excess solar radiation, extreme temperatures and desiccation at different latitudes. Indoors, the typology of the cave or the characteristics of confined environments strongly selects the microbial community according to light availability and air humidity. Interactions of cyanobacteria with rocky substrata serving as the source of mineral nutrients are based on the adhesion mechanisms and metabolic processes that allow the development of these biofilms. Both types of subaerial phototrophic community include cyanobacteria that support associated populations of heterotrophic populations of mostly very specialized species. The distribution of particular cyanobacterial taxa on monuments in urban or agricultural areas is related mostly to climatic conditions and the position and orientation of the hard surface with respect to water availability and air circulation.

81 citations


Cites background from "Cyanobacteria-containing biofilms f..."

  • ...Ramírez et al. ( 2010 ) , who studied buildings at Palenque, another archaeological site in Mexico, described the three-dimensional structure and distribution on rock, stucco and concrete of photosynthetic microorganisms in the bio fi lms dominated by the desiccation-tolerant Scytonema guyanense…...

    [...]

Journal ArticleDOI
TL;DR: Light forest cover seems beneficial for the conservation of the Angkor monuments since it reduces evaporation processes, but further studies should be carried out so as to find an optimal balance between contrasting factors.

69 citations

References
More filters
Journal ArticleDOI
TL;DR: Five species of the genera Trentepohlia and Printzina were found to occur in urban habitats in western Ireland, and reproduction took place by release of biflagellate swarmers behaving as asexual spores, germinating to produce new plants without any evidence of sexual fusion.
Abstract: On the basis of field and culture investigations, five species of the genera Trentepohlia and Printzina were found to occur in urban habitats in western Ireland: Trentepohlia abietina (Flotow) Hansgirg, T. aurea (Linnaeus) Martius, T. iolithus (Linnaeus) Wallroth, T. cf. umbrina (Kutzing) Bornet, and Printzina lagenifera (Hildebrandt) Thompson et Wujek. These species formed perennial populations on a variety of substrata. T. abietina occurred on bark of trees; T. cf. umbrina occurred on stone walls; and P. lagenifera grew on several substrata, mainly cement and asbestos sheeting. T. aurea and T. iolithus were found on old concrete and cement walls; in particular, the latter species formed characteristic, extensive, deep-red patches on many buildings. In culture, best growth and reproduction of these species were observed at 10 and 15° C, 16:8 h light:dark. Both in culture and in the field, reproduction took place by release of biflagellate swarmers behaving as asexual spores, germinating to produce new plants without any evidence of sexual fusion; release of biflagellate swarmers in the field was generally observed in all seasons throughout a whole annual cycle. Confirmation of the occurrence of sexual reproduction in Trentepohlia was not obtained.

79 citations


"Cyanobacteria-containing biofilms f..." refers background in this paper

  • ...However, their strategies to overcome the dry season appear to be different (Büdel 1999; Rindi and Guiry 2002)....

    [...]

Journal ArticleDOI
TL;DR: In situ microscopy has allowed characterization of the biofilms involved in biodeterioration processes affecting stone monuments and has revealed the biogeophysical and biogeochemical impact of the microbiota present.
Abstract: In situ microscopy consists of simultaneously applying several microscopy techniques without separating the biological component from its habitat. Over the past few years, this strategy has allowed characterization of the biofilms involved in biodeterioration processes affecting stone monuments and has revealed the biogeophysical and biogeochemical impact of the microbiota present. In addition, through in situ microscopy diagnosis, appropriate treatments can be designed to resolve the problems related to microbial colonization of stone monuments. [Int Microbiol 2005; 8(3):181-188]

73 citations


"Cyanobacteria-containing biofilms f..." refers methods in this paper

  • ...Fluorescence of photosynthetic pigments was used to compare the architecture of the biofilms and determine morphospecies, the depth at which they thrive, and whethers they were alive (Roldán et al. 2004; De los Rı́os and Ascaso 2005; Horat et al. 2006)....

    [...]

Book ChapterDOI
01 Jan 2000
TL;DR: In this article, the authors calculated the fractal dimension of the reactive surface of sediment and rock with water and atmosphere, and the weight of the living (mainly microbial) biomass of the planet was recalculated to be 1021 g instead of 1017 g, by including estimates of deep sedimentary and deep rock microbial biospheres.
Abstract: Microbial mats (or biofilms) under permanent water cover contain 95–98% biologically stabilised water at ambient temperature, while biofilms in atmospheric environments can be regarded as the maximum biomass maintaining metabolic potential in the presence of the minimum amount of water. Rock or other subaerial biofilms are made up primarily of poikilotroph micro-or-ganisms which thrive on the lowest water activity possible. Biofilms on and in rocks are the main factors in rock decay and the production of patinas, films, varnishes, crusts and stromatolites growing on and in rocks. A poikilotroph microflora is instrumental in maintaining life in truly extreme conditions and over considerable periods of time. The importance of the activity of the rock-dwelling biota and biofilms can be explained in terms of the fractal dimension of the reactive surface of sediment and rock with water and atmosphere, respectively. The weight of the living (mainly microbial) biomass of the planet is recalculated to be 1021 g instead of 1017 g, by including estimates of deep sedimentary and deep rock microbial biospheres. Poikilotroph biofilms under subaerial conditions are involved in both rock-destroying and rock-forming processes.

64 citations

Journal ArticleDOI
TL;DR: Calculations from microclimate data demonstrated that formation of dew or rime was possible and could frequently activate the cyanobacteria and may explain the younger age of microbial communities at Mt. Falconer compared to older and less active endolithic microorganisms reported earlier from Linnaeus Terrace, a higher altitude region that experiences colder, drier conditions.
Abstract: Endolithic photosynthetic microorganisms like cyanobacteria and algae are well known from savannas and deserts of the world, the high Arctic, and also Antarctic habitats like the Dry Valleys in the Ross Dependency. These endolithic microbial communities are thought to be at the limits of life with reported ages in the order of thousands of years. Here we report on an extensive chasmoendolithic cyanobacterial community inside granite rocks of Mt. Falconer in the lower Taylor Valley, Dry Valleys. On average, the cyanobacterial community was 4.49 ± 0.95 mm below the rock surface, where it formed a blue-green layer. The community was composed mainly of the cyanobacterium Chroococcidiopsis sp., with occasional Cyanothece cf. aeruginosa (Nageli) Komarek and Nostoc sp. Mean biomass was 168 ± 44 g carbon · m(-2) , and the mean chl a content was 24.3 ± 34.2 mg · m(-2) . In situ chl fluorescence measurements-a relative measure of photosynthetic activity-showed that they were active over long periods each day and also showed activity the next day in the absence of any moisture. Radiocarbon dating gave a relatively young age (175-280 years) for the community. Calculations from microclimate data demonstrated that formation of dew or rime was possible and could frequently activate the cyanobacteria and may explain the younger age of microbial communities at Mt. Falconer compared to older and less active endolithic microorganisms reported earlier from Linnaeus Terrace, a higher altitude region that experiences colder, drier conditions.

59 citations


"Cyanobacteria-containing biofilms f..." refers result in this paper

  • ...results are comparable with those of extreme habitats ranging from Antarctic communities (Büdel et al. 2008) to deserts (Garcia-Pichel and Belnap 1996; Wynn-Williams 2000)....

    [...]

  • ...These results are comparable with those of extreme habitats ranging from Antarctic communities (Büdel et al. 2008) to deserts (Garcia-Pichel and Belnap 1996; Wynn-Williams 2000)....

    [...]